Day 1 Convective Outlook NWS Storm Prediction Center Norman OK 0750 AM CDT Fri Apr 07 2017 Valid 071300Z - 081200Z ...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS OVER PARTS OF THE INTERIOR NORTHWEST AND NORTHERN ROCKIES... ...SUMMARY... A few thunderstorms associated with hail and strong wind gusts will be possible across eastern Oregon, eastern Washington, northern Idaho, and western Montana today. ...Synopsis... A high-amplitude upper-air pattern prevails over the contiguous U.S. and surroundings this morning, featuring well-defined cyclones centered over NY and offshore from OR. A positively tilted, synoptic-scale trough extending south-southwestward from the cyclone over the Northeast will move offshore from most of the Atlantic Coast through the period, and already has been preceded by a seasonally strong cold front now crossing the Bahamas. An extensive continental/polar air mass behind that front will render thunder potential negligible east of the Rockies through the period, thanks to feeble moisture and weak to no convective instability. Farther west, synoptic-scale ridging now from the southern Rockies to western Hudson Bay will move slowly eastward, reaching the southern High Plains, mid Missouri Valley and southern Hudson Bay by the end of the period. The Pacific cyclone is in the process of devolving into a open-wave trough, which will eject north-northeastward toward Vancouver Island while weakening markedly. This will occur as a mid/upper-level speed max and vorticity banner -- presently evident in moisture-channel imagery over the Pacific high seas well south of the Gulf of Alaska -- amplifies in prevailing westerlies and moves rapidly eastward. The latter perturbation will approach the CA coast at the end of the period and proceed inland early day-2. A vorticity max and related shortwave trough that already is inland over southern WA and eastern OR will eject east-northeastward across northern ID to northwestern MT through 00Z. ...Interior Northwest...Northern Rockies... Several factors will juxtapose to support thunderstorm potential today across the outlook area, with isolated severe hail and/or gusts possible: * Low-level warm advection early, followed by * Steepening of low/middle-level lapse rates related to * Diabatic surface heating behind an ongoing arc of thick mid/high cloud cover over the region, acting to weaken already minor MLCINH and * DCVA-related cooling aloft, collocated with * Thermally indirect ageostrophic circulation within the exit region of an elongated, cyclonically curved, 125-140-kt upper jet streak. Time series of forecast soundings suggest that related destabilization, atop weak but sufficient low-level moisture, will support MLCAPE up to about 250 J/kg. Except where locally modulated in the boundary layer by orographic forcing, vertical wind profiles generally should be unidirectional with around 35-45 kt effective-shear magnitudes -- mostly arising from speed shear. Lack of more robust low-level theta-e (especially on the southern end where drier air may advect northward from parts of the northern Great Basin), concerns over sufficient deep-convective coverage, and the somewhat early timing of strongest large-scale lift, combine to preclude a better-organized severe threat. ..Edwards.. 04/07/2017Read more
from SPC Forecast Products http://ift.tt/rATNzD
No comments:
Post a Comment